Friction
This movement is also known as Transform plat boundary Movement
A strike-slip fault has a shearing force, where the two blocks on either side of the fault move horizontally past each other. This type of fault is characterized by lateral movement along the fault line caused by horizontal forces.
The fault type that causes rocks to become twisted and strained when they snag each other is a strike-slip fault. In a strike-slip fault, rocks on either side of the fault move horizontally past each other, leading to twisting and straining along the fault zone. This type of movement is typical in transform plate boundaries such as the San Andreas Fault in California.
strike slip fault---------------------------------------------------------------------------------------------------------------- BITCHOSAURUS REX
Fault movement begins deep within the Earth at a point called the fault plane. This is the surface within the Earth where rocks on either side have moved relative to each other. The movement along the fault plane is what causes earthquakes.
It is a transform fault where rocks on either side of the fault move sideways past each other. This motion is caused by shearing forces that result in horizontal displacement along the fault line. Examples of transform faults include the San Andreas Fault in California.
Friction This movement is also known as Transform plat boundary Movement
Along fault lines. Major fault lines occur where the tectonic plates meet each other. The plates will either rub against each other or one will force the other underneath it, which commonly causes earthquakes.
A strike-slip fault has a shearing force, where the two blocks on either side of the fault move horizontally past each other. This type of fault is characterized by lateral movement along the fault line caused by horizontal forces.
The fault type that causes rocks to become twisted and strained when they snag each other is a strike-slip fault. In a strike-slip fault, rocks on either side of the fault move horizontally past each other, leading to twisting and straining along the fault zone. This type of movement is typical in transform plate boundaries such as the San Andreas Fault in California.
strike-slip
A reverse fault is caused by compressional forces in the Earth's crust, where rocks are pushed together, causing the overlying rock to move up and over the underlying rock along the fault plane. This results in a reverse fault where the hanging wall moves vertically upward in relation to the footwall.
No, not every force causes acceleration. For an object to accelerate, the force acting on it must not be balanced by an equal and opposite force. If the forces are balanced, the object will either remain at rest or continue moving at a constant velocity.
strike slip fault---------------------------------------------------------------------------------------------------------------- BITCHOSAURUS REX
Friction is when two objects touch each other, either smooth or rough friction causes the object to slow down. Also an unbalanced force is when the net force isn't 0 which causes a object to move and cause friction other than a balanced force is when the net force is 0.
Fault movement begins deep within the Earth at a point called the fault plane. This is the surface within the Earth where rocks on either side have moved relative to each other. The movement along the fault plane is what causes earthquakes.
Rocks on either side of a fault move along the surface of the fault.
The primary force opposing motion on faults is called friction. This friction between the rocks on either side of the fault prevents them from easily sliding past each other, building up stress until it is eventually released in the form of an earthquake.